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Classical 1/3 scaling of convection holds up to Ra = 10(15)
The global transport of heat and momentum in turbulent convection is constrained by thin thermal and viscous boundary layers at the heated and cooled boundaries of the system. This bottleneck is thought to be lifted once the boundary layers themselves become fully turbulent at very high values of th...
Αποθηκεύτηκε σε:
| Τόπος έκδοσης: | Proc Natl Acad Sci U S A |
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| Κύριοι συγγραφείς: | , , , |
| Μορφή: | Artigo |
| Γλώσσα: | Inglês |
| Έκδοση: |
National Academy of Sciences
2020
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| Θέματα: | |
| Διαθέσιμο Online: | https://ncbi.nlm.nih.gov/pmc/articles/PMC7149414/ https://ncbi.nlm.nih.gov/pubmed/32213591 https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1073/pnas.1922794117 |
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